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Chapman reaction kinetics

Notice that we have now numbered these equations from 1 to 4 and supplied the rate constants for these [Pg.81]

8 Incidentally, Professor Hites was forced to have lunch in Arrhenius house on the campus of Stockholm University as penitence for thinking that Arrhenius was Danish—he was Swedish. [Pg.81]

Strategy. Let us assume that the Earth s stratosphere is a large homogeneous compartment and that the flows of O2,0, and O3 are given by the four Chapman equations. The concentration of M (N2 and 02) is sufficiently high so that it is virtually a constant. To solve this problem, let us first set up the equations for the steady-state concentrations of O and 03 in other words, we will set up the equations for the rates of formation of O and O3 and set these rates equal to zero. Using these two expressions, we will then calculate the value of the 03 to [Pg.82]

02 ratio at 30 km and from this ratio get [03]. Remember from our previous work that at 30 km [Pg.82]

Because the concentrations of both 03 and O are not changing much as a function of time in the atmosphere, [Pg.82]


Pukhnachev (Ref 26) made a stability analysis of Chapman-Jouguet detonations to clarify the development of spinning detonations. The phenomena leading to them cannot be described by solution of simple hydrodynamic and reaction-kinetic equations for flat detonation fronts. The analysis was based on previous detonation stability analyses by Shchelkin et al with constant supersonic flow postulated along the z-axis at z <0. There is a sharp discontinuity at z=0, followed by the combustion zone. [Pg.559]

The related but, in the end, largely independent efforts of Vernon Harcourt, Dixon, Baker, and Chapman amounted to the creation of a school of reaction kinetics that went on to even greater things as the twentieth century advanced. For the first time chemistry in Oxford had become a major player on the international scene. Nothing that had been done at the centre, in the Museum, or the Old Chemistry Department as it was later called, was of the same calibre. In a lecture to mark the jubilee of the erection of the Museum in 1908 Vernon Harcourt put it more tactfully ... [Pg.120]

Figure 14.16 The balance of diffusion and surface reaction kinetics idealized depictions, (a) Surface reaction rate diffusion rate (b) Diffusion rate surface reaction rate. Source Reprinted with permission from Savage GG, Carbon-Carbon Composites, Chapman and Hall, London, 92,1992. Copyright 1992, Springer. Figure 14.16 The balance of diffusion and surface reaction kinetics idealized depictions, (a) Surface reaction rate diffusion rate (b) Diffusion rate surface reaction rate. Source Reprinted with permission from Savage GG, Carbon-Carbon Composites, Chapman and Hall, London, 92,1992. Copyright 1992, Springer.
A. K. Galwey, Reactions in the Sohd State, in Bamford and Tipper, eds.. Comprehensive Chemical Kinetics, vol. 22, Elsevier, 1980. Galwey, A. K., Chemistry of Solids, Chapman and Hall, 1967. Sohn, H. Y, and W. E. Wadsworth, eds.. Rate Frocesses of Extractive Metallurgy, Plenum Press, 1979. Szekely, J., J. W. Evans, and H. Y. Sohn, Gas-Solid Reactions, Academic Press, 1976. Uhmann, ed., Enzyklopaedie der technischen Chemie, Uncatalyzed Reactions with Solids, vol.. 3, 4th ed., Verlag Chemie, 1973, pp. 395-464. [Pg.2127]

The Chapman-Jongnet (CJ) theory is a one-dimensional model that treats the detonation shock wave as a discontinnity with infinite reaction rate. The conservation equations for mass, momentum, and energy across the one-dimensional wave gives a unique solution for the detonation velocity (CJ velocity) and the state of combustion products immediately behind the detonation wave. Based on the CJ theory it is possible to calculate detonation velocity, detonation pressure, etc. if the gas mixtnre composition is known. The CJ theory does not require any information about the chemical reaction rate (i.e., chemical kinetics). [Pg.67]

From the standpoint of geometrical considerations, the major difference is in the far greater steric requirements of the nitro group. This could result in either primary or secondary steric effects. Nevertheless, primary steric effects do not seem to be necessarily distinguishable by direct kinetic comparison. A classic example is the puzzling similarity of the activation parameters of 2-chloropyrimidine and 2,6-dinitrochlorobenzene (reaction with piperidine in ethanol), which has been described by Chapman and Rees as fortuitous. However, that nitro groups do cause (retarding) primary steric effects has been neatly shown at peri positions in the reaction with alkoxides (see Section IV,C, l,c). [Pg.321]

It should be pointed out that the existence of stable structures of the intermediate-complex type (also known as a-complexes or Wheland complexes) is not of itself evidence for their being obligate intermediates in aromatic nucleophilic substitution. The lack of an element effect is suggested, but not established as in benzene derivatives (see Sections I,D,2 and II, D). The activated order of halogen reactivity F > Cl Br I has been observed in quantita-tivei36a,i37 Tables II, VII-XIII) and in many qualitative studies (see Section II, D). The reverse sequence applies to some less-activated compounds such as 3-halopyridines, but not in general.Bimolecular kinetics has been established by Chapman and others (Sections III, A and IV, A) for various reactions. [Pg.170]

In spite of the extensive kinetic work of Chapman and co-workers, much remains to be done on the reactivity of azines with nucleophiles. The data available on substitution by alkoxide ions are especially meager. The missing information on alkoxide reactions should give a better picture of the activation of different ring-positions than is possible with the data on aminations. The latter include the effects shown in 235, 276, and 277 in addition to activation by the azine-nitrogens. [Pg.269]

Catalytic reactions (as well as the related class of chain reactions described below) are coupled reactions, and their kinetic description requires methods to solve the associated set of differential equations that describe the constituent steps. This stimulated Chapman in 1913 to formulate the steady state approximation which, as we will see, plays a central role in solving kinetic schemes. [Pg.23]

These modifications are known as the Frumkin double-layer corrections. They are useful when the electrolyte concentration is sufficiently low, so that fa can be calculated from Gouy-Chapman theory, and the uncertainty in the position of the reaction site is unimportant. Whenever possible, kinetic investigations should be carried out with a high concentration of supporting electrolyte, so that double-layer corrections can be avoided. [Pg.63]

A purely thermodynamic treatment of detonation ignores the important question of reaction time scales. The finite time scale of reaction leads to strong deviations in detonation velocities from values based on the Chapman-Jouguet theory.16 The kinetics of even simple molecules under high-pressure conditions is not well understood. [Pg.162]

In Vaughan, D.J. Pattrick, R.A.D. (eds.) Mineral Surfaces. Min. Soc. Series 5, Chapman Hall, London, 129-183 Brown, WE.B. Dollimore, D. Galwey A.K. (1980) Reactions in the solid state. In Barn-ford, C.H. Tipper, C.F.H. (eds.) Comprehensive chemical kinetics. Elsevier Amsterdam, 22 41-109... [Pg.564]

As for the quasi (pseudo)-steady-state case, the basic assumption in deriving kinetic equations is the well-known Bodenshtein hypothesis according to which the rates of formation and consumption of intermediates are equal. In fact. Chapman was first who proposed this hypothesis (see in more detail in the book by Yablonskii et al., 1991). The approach based on this idea, the Quasi-Steady-State Approximation (QSSA), is a common method for eliminating intermediates from the kinetic models of complex catalytic reactions and corresponding transformation of these models. As well known, in the literature on chemical problems, another name of this approach, the Pseudo-Steady-State Approximation (PSSA) is used. However, the term "Quasi-Steady-State Approximation" is more popular. According to the Internet, the number of references on the QSSA is more than 70,000 in comparison with about 22,000, number of references on PSSA. [Pg.49]

Ahrland, S. Solution Chemistry and Kinetics of Ionic Reactions. In The Chemistry of Actinide Elements. (Edit. Katz, J.J. Seaborg, G.T. Morris, L.R.) Chapman Hall London, 1986, vol. 2, chap. 21, p. 1480. [Pg.489]

Chapman and his co-workers have concluded that the reversibility of several of these reactions is not significant enough to be included in the kinetic considerations. Radioactive isotopes could be used to measure the degree of reversibility, even if very low, and kinetic parameters on the reverse substitution process could also be obtained. [Pg.278]

The rates of reactions (149)-(152) vary with altitude. The rate constants of reactions (149) and (151) are determined by the solar flux at a given altitude, and the rate constants of the other reactions are determined by the temperature at that altitude. However, precise solar data obtained from rocket experiments and better kinetic data for reactions (150)-( 152), coupled with recent meteorological analysis, have shown that the Chapman model was seriously flawed. The concentrations predicted by the model were essentially too high. Something else was affecting the ozone. [Pg.425]

The end result of the Chapman mechanism, and of the modified Chapman processes as elucidated by later investigators" "" is that sodium and other metals (if Chapman-like mechanisms hold for the other metals) are abundant in atomic form. The kinetic studies show that molecular compounds are not present in large quantities above 85 km. Further work " showed that following the formation of dense atomic trails during the vaporization process, molecular recombination in the wake occurs to form smoke or dust that can then act as a delayed source of sodium (and other) atoms. It was then suggested that NaO reacts with atmospheric H2O to form gaseous NaOH, with the latter reacting with atmospheric CO2 in a three-body reaction to form NaHCOs" ... [Pg.290]


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See also in sourсe #XX -- [ Pg.81 ]




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